Compensation method and sensitivity analysis of DPHP frozen soil ice content measurement

IF 0.7 4区 地球科学 Q4 GEOGRAPHY, PHYSICAL
YongMing Cai , Meng Wang , Xu Li , WenHua Chen
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Abstract

The Duel-Probe-Heat-Pulse (DPHP) ice content sensor can measure the ice content of the soil, but its measurement process is not clear for the disturbance of frozen soil. In this study, the ice content measurement test was carried out for silty clay specimens. Firstly, the influence of heating power was clarified. The variation trends of the temperature rise relaxation area in the respective conditions of the three representative volumetric water content specimens and the degree of compaction of the specimen preparation was compared. Then, the influence of five kinds of heating interval time on the measurement accuracy was explored. Finally, the compensation and analysis method of the temperature relaxation area, based on the temperature of the measuring point and the phase change of ice water, is proposed. The experimental results show that: (1) There is a hysteresis in the temperature rise curve of the probe of the DPHP ice content sensor. In the measurement process, a long enough integral interval should be selected to calculate the temperature relaxation area. (2) For the specimens with the same initial water content, the measured temperature relaxation area increases with the increase of compaction degree, and this trend weakens in the specimens with the increase of water content. (3) The DPHP ice content sensor causes irreversible disturbance to the soil during the measurement process. The temperature relaxation area, obtained by continuous measurement at a short heating interval, is small, and manifests a decreasing trend with the increase of measurement times. (4) It is recommended that the heating interval time should be more than 120 min, and the temperature relaxation area should be compensated when the continuous measurement of short heating interval time is carried out, to offset the influence of the temperature rise of the measuring point. The research results reveals the influence of multiple factors on the measurement of DPHP ice content sensors, which can provide a basis for the accuracy of soil ice content measurement.
DPHP冻土冰含量测量的补偿方法及灵敏度分析
双探头-热脉冲(dual - probe - heat - pulse, DPHP)冰含量传感器可以测量土壤的冰含量,但由于冻土的扰动,其测量过程不明确。本研究对粉质粘土试样进行了含冰量测量试验。首先,阐明了加热功率的影响。比较了三种具有代表性的体积含水量试样在各自条件下的温升松弛区变化趋势及制样压实程度。然后,探讨了五种加热间隔时间对测量精度的影响。最后,提出了基于测点温度和冰水相变的温度松弛区补偿分析方法。实验结果表明:(1)DPHP冰含量传感器探头温升曲线存在滞后。在测量过程中,应选择足够长的积分区间来计算温度松弛区。(2)对于初始含水量相同的试样,实测温度松弛面积随压实程度的增加而增大,且随含水量的增加而减弱。(3) DPHP冰含量传感器在测量过程中会对土壤产生不可逆的扰动。在较短的加热间隔内连续测量得到的温度松弛区较小,且随测量次数的增加呈减小趋势。(4)建议加热间隔时间应大于120min,进行短加热间隔时间的连续测量时,应补偿温度松弛区,以抵消测点温升的影响。研究结果揭示了多种因素对DPHP冰含量传感器测量的影响,可为土壤冰含量测量的准确性提供依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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CiteScore
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